Academic literature on the topic 'Aeromagnetic analysis'

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Journal articles on the topic "Aeromagnetic analysis"

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Wu, Peilin, Qunying Zhang, Luzhao Chen, Wanhua Zhu, and Guangyou Fang. "Aeromagnetic Compensation Algorithm Based on Principal Component Analysis." Journal of Sensors 2018 (2018): 1–7. http://dx.doi.org/10.1155/2018/5798287.

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Aeromagnetic exploration is an important exploration method in geophysics. The data is typically measured by optically pumped magnetometer mounted on an aircraft. But any aircraft produces significant levels of magnetic interference. Therefore, aeromagnetic compensation is important in aeromagnetic exploration. However, multicollinearity of the aeromagnetic compensation model degrades the performance of the compensation. To address this issue, a novel aeromagnetic compensation method based on principal component analysis is proposed. Using the algorithm, the correlation in the feature matrix is eliminated and the principal components are using to construct the hyperplane to compensate the platform-generated magnetic fields. The algorithm was tested using a helicopter, and the obtained improvement ratio is 9.86. The compensated quality is almost the same or slightly better than the ridge regression. The validity of the proposed method was experimentally demonstrated.
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Hansen, R. O., and Eduard deRidder. "Linear feature analysis for aeromagnetic data." GEOPHYSICS 71, no. 6 (November 2006): L61—L67. http://dx.doi.org/10.1190/1.2357831.

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This paper presents a new approach to detecting and two approaches to displaying lineaments associated with high-angle magnetic contacts, based on analysis of the curvature of the total horizontal gradient of the total magnetic field reduced to the pole. The first display is a contour or color plot of minus the principal curvature of largest absolute value. The second is a point plot of the local maxima of minus the largest principal curvature in regions where this curvature is negative. The paper also develops a depth-estimation technique for magnetic contacts based on the ratio of the curvature of the total gradient to the total gradient itself. Tests on synthetic data yield excellent results in detecting and delineating magnetic contact edges, and reasonable performance in producing depth estimates for the magnetic contacts. Results obtained using aeromagnetic data from the Finger Lakes region of New York State show good correlation with known structural features.
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Cooper, G. R. J. "The antialiased textural analysis of aeromagnetic data." Computers & Geosciences 35, no. 3 (March 2009): 586–91. http://dx.doi.org/10.1016/j.cageo.2008.04.009.

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Arogundade, Augustine Babatunde, Olaide Sakiru Hammed, Musa Olufemi Awoyemi, Sesan Cornelius Falade, Ojudoo Darius Ajama, Folarin Adisa Olayode, Adebiyi Samuel Adebayo, and Ayomide Oluyemi Olabode. "Analysis of aeromagnetic anomalies of parts of Chad Basin, Nigeria, using high-resolution aeromagnetic data." Modeling Earth Systems and Environment 6, no. 3 (April 23, 2020): 1545–56. http://dx.doi.org/10.1007/s40808-020-00769-y.

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Gruzdev, R. "Magnetic survey – ground technology, aeromagnetic survey on aircraft and unmanned aerial vehicles: a comparative analysis of the results (on the example of Eastern Transbaikalia)." Transbaikal State University Journal 26, no. 8 (2020): 6–15. http://dx.doi.org/10.21209/2227-9245-2020-26-8-6-15.

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The use of unmanned aerial vehicles (UAVs) in geophysical work is becoming a very popular area in the field of modern geological exploration. The advantage of unmanned systems is the optimal ratio of the quality of research results with a significant increase in work productivity and a decrease in cost. In this regard, the improvement of field techniques and the processing of UAV materials is of particular interest for exploration. On the subject, there are a number of unresolved issues that have been revealed to some extent as a result of the author’s comparison of ground-based magnetic exploration and aeromagnetic survey data. The purpose of the study was to assess the possibility of a full-fledged replacement of ground magnetic exploration work for aeromagnetic survey using unmanned aerial vehicles. The comparison of different types of magnetic survey is relevant, since on the basis of the actual material, the possibility of using an alternative more productive method – aeromagnetic survey using modern UAVs – instead of traditional expensive ground-based magnetic exploration works is analyzed. To compare the results of the studies, actual material obtained from field work on an area of 13,4 km2 was used. Based on the databases, maps of anomalous magnetic field and graphs on several geophysical profiles are built. Results of magnetic survey in air and ground versions are analyzed; correlation relationships between data of ground pedestrian magnetic survey and aeromagnetic system on An-3 and UAV aircraft are established. Based on the results of the study, correlation and determination coefficients were obtained, which indicate that geophysical methods on UAVs adequately occupy their place between classical aerogeophysics and ground-based pedestrian survey. Moreover, aeromagnetic survey using UAVs is able to replace pedestrian magnetic exploration during work at the same heights. Based on the results of the study, methodological recommendations for the production of aeromagnetic survey on UAVs were compiled
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Lee, Madeline, and William Morris. "Quality assurance of aeromagnetic data using lineament analysis." Exploration Geophysics 44, no. 2 (June 2013): 104–13. http://dx.doi.org/10.1071/eg12034.

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Holden, Eun-Jung, Mike Dentith, and Peter Kovesi. "Automatic Analysis of Aeromagnetic Images for Gold Exploration." ASEG Extended Abstracts 2007, no. 1 (December 1, 2007): 1–4. http://dx.doi.org/10.1071/aseg2007ab057.

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Kivior, I., and D. Boyd. "THE INTERPRETATION OF AEROMAGNETIC SURVEYS FOR HYDROCARBON EXPLORATION." APPEA Journal 39, no. 1 (1999): 494. http://dx.doi.org/10.1071/aj98030.

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Aeromagnetic surveys have been generally regarded in petroleum exploration as a reconnaissance tool for major structures. They were used commonly in the early stages of exploration to delineate the shape and depth of the sedimentary basin by detecting the strong magnetic contrast between the sediments and the underlying metamorphic basement. Recent developments in the application of computer technology to the study of the earth's magnetic field have significantly extended the scope of aeromagnetic surveys as a tool in the exploration for hydrocarbons. In this paper the two principal methods used in the analysis and interpretation of aeromagnetic data over sedimentary basins are: 1) energy spectral analysis applied to gridded data; and, 2) automatic curve matching applied to profile data. It is important to establish the magnetic character of sedimentary and basement rocks, and to determine the regional magnetic character of the area by applying energy spectral analysis. Application of automatic curve matching to profile data can provide results from the sedimentary section and deeper parts of a basin. High quality magnetic data from an experimental aeromagnetic survey flown over part of the Eromanga/Cooper Basin has recently been interpreted using this new approach. From this survey it is possible to detect major structures such as highs and troughs in the weakly magnetic basement, as well as pick out faults, and magnetic layers in the sedimentary section. The results are consistent with interpretation from seismic and demonstrate that aeromagnetic data can be used to assist seismic interpretation, for example to interpolate between widely spaced seismic lines and sometimes to locate structures which can not be detected from seismic surveys. This new approach to the interpretation of aeromagnetic data can provide a complementary tool for hydrocarbon exploration, which is ideal for logistically difficult terrain and environmentally sensitive areas.
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Eaton, D., and K. Vasudevan. "Skeletonization of aeromagnetic data." GEOPHYSICS 69, no. 2 (March 2004): 478–88. http://dx.doi.org/10.1190/1.1707068.

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Skeletonization is a syntactic pattern‐recognition method that is applied to gridded data to produce an automatic line drawing, with an associated event catalog. Previous implementations of skeletonization have been tailored for seismic data. Here, we modify that technique to render it more suitable for other types of gridded data, with particular emphasis on aeromagnetic maps. A modification from previous schemes is the use of a two‐pass approach, to reduce the effects of an otherwise problematic directional bias that discriminates against events oriented parallel to columns of the grid. The method can be used effectively for filtering aeromagnetic data on the basis of strike direction, event linearity, event amplitude, and polarity. It is based on the delineation of peak‐trough pairs (cycles), which are traced throughout the grid to form contiguous events. Cycles and events are characterized by attributes that include amplitude, polarity, and pulse width. Events are further characterized by length, average strike direction, and linearity. The event attributes are stored in a catalog, thus enabling one to perform attribute‐based analysis and data filtering. We illustrate our algorithm using two regional aeromagnetic examples from different parts of the Canadian Shield. The first, from the Great Slave Lake shear zone, is dominated by linear anomaly trends produced by faults and mafic dikes. The second, from the Manicouagan region of northeastern Quebec, contains abundant subcircular and arcuate anomaly patterns caused by large intrusive complexes and a meteorite impact structure.
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Dahuwa, Dahiru, Yusuf Abubakar Sanusi, Emmanuel Emeka Udensi, and Musa Momoh. "The Analysis of Aeromagnetic Data overWaseand It Adjoining Area." IOSR Journal of Applied Physics 08, no. 04 (April 2016): 57–66. http://dx.doi.org/10.9790/4861-0804015766.

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Dissertations / Theses on the topic "Aeromagnetic analysis"

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Lucius, Jeffrey E. "Crustal geology of Ohio inferred from aeromagnetic and gravity anomaly analysis." The Ohio State University, 1985. http://rave.ohiolink.edu/etdc/view?acc_num=osu1318868502.

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Leblanc, G. "Wavelet analysis denoising of aeromagnetic data, application to hydrocarbon and mineral exploration." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0035/NQ66216.pdf.

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Martin, J. E. "Spectral analysis of aeromagnetic data and investigation of errors in spherical harmonic models." Thesis, University of Newcastle Upon Tyne, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.376255.

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Santamaria, Vallejos Luis E. "Three-dimensional analysis of aeromagnetic and gravimetric data of sedimentary basins from Panama, Central America /." Luleå : Luleå University of Technology, 2008. http://epubl.ltu.se/1402-1757/2008/24/.

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Vallejos, Luis E. Santamaria. "Three-dimensional analysis of aeromagnetic and gravimetric data of sedimentary basins from Panama, Central America." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-18258.

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The knowledge of the geology of the sedimentary basins from the Gulf of Panama is still quite limited. There is a lack of data from the basin geometry, the thickness, the continuity and connection between the basins, and from the characteristics of the crystalline basement rocks beneath the sedimentary basins. Geological maps have been published without evidence from geophysical studies; i.e. marine faults patters are showed only as the continuation of fault pattern on land and in some cases faults are showed only to adjust geodynamics models. In the marines areas the geophysical surveys so far carried out, like seismic reflection and well logging, have not given information about the nature of and depth to the crystalline basement rock and interpretations of aeromagnetic and gravity data are still missing. Many of the geophysical surveys like aeromagnetic and marine gravity data have been published as contour maps. However, different data processing techniques and various references levels have been used, which do not permit an integral regional analysis. Here we present composite regional aeromagnetic and gravity maps and integral interpretations with reference to source parameters such as; depths to the top of basement rock, faults patters, locations of magnetic boundaries, susceptibility contrasts, geometry and connection between the basins. The interpretations are based on regional aeromagnetic maps and on marine and land gravity data compiled from several sources and integrated with reference to a fixed level. Various techniques have been applied for the interpretation e.g. enhancement of the aeromagnetic anomalies maps by sun shading technique, applying band pass filtering and upward analytic continuation. Maps have also been transformed into images called 3D analytic signal amplitude and local wave number maps. The depth estimates resulting from the analyses of these maps are compared and the location of interpreted contacts are combined into a map showing the dip direction for contacts. The Bouguer gravity data from the Gulf of Panama are transformed into a residual anomaly map using a filtering technique. This residual anomaly map have been analyzed in order to estimate depths to the top of the basement rocks.

Godkänd; 2008; 20080602 (ysko)

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Leonard, Mark. "Interpretation of an aeromagnetic survey over a shallow sedimentary basin with particular emphasis on spectral analysis /." Title page, contents and abstract only, 1986. http://web4.library.adelaide.edu.au/theses/09SB/09sbl581.pdf.

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Magaia, Luis. "Processing Techniques of Aeromagnetic Data. Case Studies from the Precambrian of Mozambique." Thesis, Uppsala universitet, Geofysik, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-183714.

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During 2002-2006 geological field work were carried out in Mozambique. The purpose was to check the preliminary geological interpretations and also to resolve the problems that arose during the compilation of preliminary geological maps and collect samples for laboratory studies. In parallel, airborne geophysical data were collected in many parts of the country to support the geological interpretation and compilation of geophysical maps. In the present work the aeromagnetic data collected in 2004 and 2005 in two small areas northwest of Niassa province and another one in eastern part of Tete province is analysed using GeosoftTM. The processing of aeromagnetic data began with the removal of diurnal variations and corrections for IGRF model of the Earth in the data set. The study of the effect of height variations on recorded magnetic field, levelling and interpolation techniques were also studied. La Porte interpolation showed to be a good tool for interpolation of aeromagnetic data using measured horizontal gradient. Depth estimation techniques are also used to obtain semi-quantitative interpretation of geological bodies. It was showed that many features in the study areas are located at shallow depth (less than 500 m) and few geological features are located at depths greater than 1000 m. This interpretation could be used to draw conclusions about the geology or be incorporated into further investigations in these areas.
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Le, Maire Pauline. "Caractérisation des anomalies magnétiques, approches théoriques et expérimentales : applications à des objets anthropiques et géologiques." Thesis, Strasbourg, 2017. http://www.theses.fr/2017STRAH006/document.

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L’objectif de ce travail est d’améliorer la caractérisation des sources à l’origine d’anomalies magnétiques, par le biais de développements théoriques et expérimentaux. Pour des structures invariantes dans une direction horizontale (structures à 2D), l’idée de Nabighian (1972) a été généralisée, ce qui implique une nouvelle façon d’étudier les méthodes potentielles à 2D. Ces développements ont permis de proposer une nouvelle approche théorique et de nouvelles représentations dans le plan complexe des fonctions magnétiques. La deuxième approche de ce travail est expérimentale. Une étude y est faite par le biais de données et de cas synthétiques, afin d’estimer l’apport d’acquisitions magnétiques à différentes altitudes pour caractériser une source. Dans un troisième temps, les développements théoriques et expérimentaux sont mis en œuvre pour deux exemples : des anomalies magnétiques en domaine océanique de type Vine et Mathews et une cartographie pour l’archéologie
Magnetic anomalies recorded outside bodies provide high quality information relative to buried structures. By using theoretical and experimental developments, this thesis aims to improve the characterization of the source inducing the magnetic anomaly. Firstly, some properties of three dimensional magnetic functions are presented, for example the presence of several maxima of the analytic signal operator (3D) is demonstrated. The Nabighian (1972) equation is generalized, which imply a new process to study potential method in two dimensions. These developments enable a new visualization of the anomaly in the complex field. The second approach is experimental. Synthetic cases are used to estimate the contribution of different configurations of magnetic data acquisitions at different altitudes to characterize the magnetic source. Theoretical and experimental developments are finally applied to two field examples: oceanic magnetic anomalies and archaeological magnetic prospection
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Books on the topic "Aeromagnetic analysis"

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McCormick, Kelli A. Drilling of an aeromagnetic anomaly in southeastern South Dakota: Results from analysis of paleozoic and precambrian core. Vermillion, S.D: University of South Dakota, Akeley-Lawrence Science Center, 2005.

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Langenheim, Victoria E. Geophysical framework based on analysis of aeromagnetic and gravity data, upper and middle Verde River watershed, Yavapai County, Arizona. Reston, Va: U.S. Geological Survey, 2005.

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Langel, R. A. Geodynamics branch data base for main magnetic field analysis. Greenbelt, MD: Goddard Space Flight Center, 1991.

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Locations, descriptions, densities, and magnetic susceptibilities of rock samples collected for analyses of gravity and aeromagnetic anomalies in Yellowstone National Park, Wyoming, Idaho, and Montana. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Locations, descriptions, densities, and magnetic susceptibilities of rock samples collected for analyses of gravity and aeromagnetic anomalies in Yellowstone National Park, Wyoming, Idaho, and Montana. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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L, Christiansen Robert, and Geological Survey (U.S.), eds. Locations, descriptions, densities, and magnetic susceptibilities of rock samples collected for analyses of gravity and aeromagnetic anomalies in Yellowstone National Park, Wyoming, Idaho, and Montana. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Book chapters on the topic "Aeromagnetic analysis"

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Abraham, Ema M., and Onyekachi E. Itumoh. "Geothermal Reconnaissance of Southeastern Nigeria from Analysis of Aeromagnetic Data." In On Significant Applications of Geophysical Methods, 43–46. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01656-2_9.

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Longo, L. M., R. Ritis, G. Ventura, and M. Chiappini. "Analysis of the Aeromagnetic Anomalies of the Auca Mahuida Volcano, Patagonia, Argentina." In Pageoph Topical Volumes, 3273–90. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-51529-8_4.

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"4. Structural analysis from aeromagnetic data." In Geological Interpretation of Aeromagnetic Data, 63–93. Society of Exploration Geophysicists and Australian Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/1.9781560803218.ch4.

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Berger, Zeev, Jim Davies, and Robin T. Thompson. "Integrated Analysis of High-resolution Aeromagnetic (HRAM) and RADARSAT-1 Imagery for Exploration in Mature and Frontier Basins." In Surface Exploration Case HistoriesApplications of Geoschemistry, Magnetics, and Remote Sensing. American Association of Petroleum Geologists, 2002. http://dx.doi.org/10.1306/st48794c13.

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Conference papers on the topic "Aeromagnetic analysis"

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Cooper, Gordon R. J. "A new semiautomatic interpretation technique for aeromagnetic data." In PROCEEDINGS OF THE INTERNATIONAL CONFERENCE ON NUMERICAL ANALYSIS AND APPLIED MATHEMATICS 2014 (ICNAAM-2014). AIP Publishing LLC, 2015. http://dx.doi.org/10.1063/1.4913063.

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Paoletti, V., M. Fedi, G. Florio, A. Rapolla, and R. Supper. "Analysis of Aeromagnetic Data Affected by Intense Cultural Noise." In 65th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.6.e33.

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Boubekri, Hichem, Mohamed Hamoudi, and Sid-Ali Ouadfeul. "STATISTICAL CROSS CORRELATION ANALYSIS FOR AEROMAGNETIC FIELD VECTOR DETERMINATION." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2013. Environment and Engineering Geophysical Society, 2013. http://dx.doi.org/10.4133/sageep2013-035.1.

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boufkri, hafsa, Driss El Azzab, Abdelhalim Miftah, and Mohammed Charroud. "Processing and Analysis of aeromagnetic data of North-Eastern Morocco." In The 2nd International Electronic Conference on Mineral Science. Basel, Switzerland: MDPI, 2021. http://dx.doi.org/10.3390/iecms2021-09367.

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Holden, Eun-Jung, Peter Kovesi, Mike C. Dentith, Daniel Wedge, Jason C. Wong, and Shih Ching Fu. "Detection of regions of structural complexity within aeromagnetic data using image analysis." In 2010 25th International Conference of Image and Vision Computing New Zealand (IVCNZ). IEEE, 2010. http://dx.doi.org/10.1109/ivcnz.2010.6148856.

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Walter, Callum, Alexander Braun, and Georgia Fotopoulos. "Spectral Analysis of Magnetometer Swing in High-Resolution UAV-borne Aeromagnetic Surveys." In 2019 IEEE Systems and Technologies for Remote Sensing Applications Through Unmanned Aerial Systems (STRATUS). IEEE, 2019. http://dx.doi.org/10.1109/stratus.2019.8713313.

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Ouadfeul, Sid-Ali, Leila Aliouane, and Said Eladj. "Wavelet analysis of 3D Analytic singal for contacts identification from aeromagnetic data." In 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15-18 August 2011. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2011. http://dx.doi.org/10.1190/sbgf2011-144.

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Xu, Shi, Hui Wang, Jingshui Kuang, Yong Wang, Wei Zheng, and Hailong Sun. "The analysis of aeromagnetic survey physical background about somewhere in Qinling Mountains." In MATHEMATICAL SCIENCES AND ITS APPLICATIONS. Author(s), 2017. http://dx.doi.org/10.1063/1.4971928.

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Jirigalatu, J., A. Døssing Andreasen, and E. Lima Simões da Silva. "Noise Analysis of a Portable Aeromagnetic Surveying System Using a Hybrid UAV." In NSG2020 3rd Conference on Geophysics for Mineral Exploration and Mining. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202020083.

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Brandsberg-Dahl, S., J. Dellinger, R. Clarke, and L. Thomsen. "Analysis of High Resolution Aeromagnetic Anomalies from the South-Central Alberta Foothills, Canada." In 65th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.6.g044.

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Reports on the topic "Aeromagnetic analysis"

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Nelson, B., D. Hardwick, D. Forsyth, M. Bower, D. Marcotte, M. Macpherson, R. Macnab, and D. Teskey. Preliminary Analysis of Data From the Lincoln Sea Aeromagnetic Surveys 1989 - 1990. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132542.

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Aeromagnetic map and analysis of aeromagnetic and aeroradioactivity data in the Blood Mountain, Chattahoochee, and Tray Mountain Roadless Areas, northern Georgia. US Geological Survey, 1985. http://dx.doi.org/10.3133/mf1347e.

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